A theory of how the sun creates heat: when sunlight interacts with something, it makes it vibrate. At sea level, all the heavy molecules are, like O2. The heavier a molecule is, the more energy it produces once it vibrates, which we experienced as heat. 1000 meters over sea level, the air is thinner, less heavy molecules are here, producing less energy ones sunlight interacts with it, making it colder the higher up in the air you go.
Yes. The closer you are to the sun, at sea level, the hotter it gets. The further away you are from the sun at sea level, the colder it gets. In December, the Arctic experience little to no sun light, making water at sea level to freeze; in June, the Arctic experience 24 hours sunlight, making the ice at sea level to melt.
The sun moves in a circular path above our head. The Arctic is inside the circular path of the sun, while the Antarctica is outside the circular path of the sun. The outside circular path (Antarctica) makes a much bigger circle around the earth, then the inside circular path (Arctic). If you are inside or outside the circular path the sun makes, once you get far enough away from the sun, it will get dark outside, as sunlight no longer reaches you, making it cold, and water at sea level turn to a solid form, known as ice.
Two places will ice form in a circular shape. One at the centre of the earth, that be the Arctic. The other at the edge of the known earth, known as the Antarctica, which makes a much bigger ice circle.
A theory of how the sun creates heat: when sunlight interacts with something, it makes it vibrate. At sea level, all the heavy molecules are, like O2. The heavier a molecule is, the more energy it produces once it vibrates, which we experienced as heat. 1000 meters over sea level, the air is thinner, less heavy molecules are here, producing less energy ones sunlight interacts with it, making it colder the higher up in the air you go.
Yes. The closer you are to the sun, at sea level, the hotter it gets. The further away you are from the sun at sea level, the colder it gets. In December, the Arctic experience little to no sun light, making water at sea level to freeze; in June, the Arctic experience 24 hours sunlight, making the ice at sea level to melt.
The sun moves in a circular path above our head. The Arctic is inside the circular path of the sun, while the Antarctica is outside the circular path of the sun. The outside circular path (Antarctica) makes a much bigger circle around the earth, then the inside circular path (Arctic). If you are inside or outside the circular path the sun makes, once you get far enough away from the sun, it will get dark outside, as sunlight no longer reaches you, making it cold, and water at sea level turn to a solid form, known as ice.
Two places will ice form in a circular shape. One at the centre of the earth, that be the Arctic. The other at the edge of the known earth, known as the Antarctica, which makes a much bigger ice circle.